高邮凹陷黄珏-马家嘴地区戴南组重力流沉积及其成因

马文睿; 傅强; 谭思哲

doi:10.3799/dqkx.2014.057

Volume 39 Issue 5

May 2014

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Article Navigation > Earth Science > 2014 > 39(5): 601-610

Ma Wenrui, Fu Qiang, Tan Sizhe, 2014. Gravity Flow Deposits and Its Genetic Mechanism of Dainan Formation in Huangjue-Majiazui District, Gaoyou Subbasin. Earth Science, 39(5): 601-610. doi: 10.3799/dqkx.2014.057

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Ma Wenrui, Fu Qiang, Tan Sizhe, 2014. Gravity Flow Deposits and Its Genetic Mechanism of Dainan Formation in Huangjue-Majiazui District, Gaoyou Subbasin. Earth Science, 39(5): 601-610. doi: 10.3799/dqkx.2014.057

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Gravity Flow Deposits and Its Genetic Mechanism of Dainan Formation in Huangjue-Majiazui District, Gaoyou Subbasin

doi: 10.3799/dqkx.2014.057

1.
School of Ocean and Earth Science, Tongji University, Shanghai 200092, China
2.
CNOOC China Ltd. Shanghai Branch, Shanghai 200030, China

Received Date: 2013-12-01
Publish Date: 2014-05-01

Abstract

Abstract

The main exploration targets of petroleum prospecting in Subei Basin shift gradually from structural reservoirs to subtle reservoirs nowadays. As potential gas and oil-bearing reservoirs, gravity flow sediment prospecting becomes more important for subtle reservoirs exploration. Based on the core observation, well logging, seismic profile characters, gravity flow deposits developed in E₂d of Huangjue-Majiazui district in Gaoyou sag and their genies are studied. It is found that nearshore subaqueous alluvial fans and slump-turbidities developed in E₂d₁ in study area, while fan deltas and slump-turbidities developed in E₂d₂. The development of sandbodies is considered to be closely coordinated with the special structural pattern, special and active tectonic backgrounds. Discovery of slump-turbidities provides theoretical framework for oil and gas exploration.
- Gaoyou subbasin,
- Huangjue-Majiazui district,
- Dainan Formation,
- gravity flow deposit,
- genesis mechanism of sandbodies,
- petroleum prospecting

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Gravity Flow Deposits and Its Genetic Mechanism of Dainan Formation in Huangjue-Majiazui District, Gaoyou Subbasin

doi: 10.3799/dqkx.2014.057

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